Geomagnetic Field Intensity during the Neolith in the Central East European Plain


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The conducted archeomagnetic studies resulted in data on variations in the geomagnetic field intensity in the central East European Plain (Sakhtysh I site area, ϕ = 56°48′ N, λ = 40°33′ E) during the time interval of 5–3 ka BC. The geomagnetic field intensity varied mainly within the range of 30–60 μT. In the first half of the 5th millennium BC, the mean level of geomagnetic field intensity was about 35 μT. In the second half of the 5th–early 4th millennium BC, it rose to about 50 μT and then decreased again to reach a mean value of about 40 μT in the period of 4–3 ka BC. Comparison of the geomagnetic field intensity variation based on the obtained data and the data on the Caucasus region for the same time interval demonstrates a certain similarity.

Sobre autores

I. Nachasova

Schmidt Institute of Physics of the Earth

Email: pilipenko@ifz.ru
Rússia, Moscow

O. Pilipenko

Schmidt Institute of Physics of the Earth

Autor responsável pela correspondência
Email: pilipenko@ifz.ru
Rússia, Moscow

G. Markov

Schmidt Institute of Physics of the Earth

Email: pilipenko@ifz.ru
Rússia, Moscow

S. Gribov

Borok Geophysical Observatory

Email: pilipenko@ifz.ru
Rússia, Borok, Yaroslavl oblast

Yu. Tsetlin

Institute of Archeology

Email: pilipenko@ifz.ru
Rússia, Moscow

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